Standing stone

A menhir (from Brittonic languages: maen or men, "stone" and hir or hîr, "long"), standing stone, orthostat, lith or masseba/matseva is a large upright standing stone. Menhirs may be found solely as monoliths, or as part of a group of similar stones. Their size can vary considerably, but their shape is generally uneven and squared, often tapering towards the top. Menhirs are widely distributed across Europe, Africa and Asia. However, they are most numerous in Western Europe; in particular in Ireland, Great Britain and Brittany. There are about 50,000 megaliths in these areas, while there are 1,200 menhirs in northwest France alone. Standing stones are usually difficult to date, but pottery, and/or pottery shards found underneath some in Atlantic Europe connects them with the Beaker people. They were constructed during many different periods across pre-history as part of a larger megalithic culture that flourished in Europe and beyond.

Some menhirs have been erected next to buildings that often have an early or current religious significance. One example is the South Zeal Menhir in Devon, which formed the basis for a 12th-century monastery built by lay monks. The monastery later became the Oxenham Arms hotel, at South Zeal, and the standing stone remains in place in the ancient snug bar at the hotel.

Where menhirs appear in groups, often in a circular, oval, henge or horseshoe formation, they are sometimes called megalithic monuments. These are sites of ancient religious ceremonies, sometimes containing burial chambers. The exact function of menhirs has provoked more debate than practically any other issue in European pre-history. Over the centuries, they have variously been thought to have been used by Druids for human sacrifice, used as territorial markers, or elements of a complex ideological system, or functioned as early calendars. Until the nineteenth century, antiquarians did not have substantial knowledge of prehistory, and their only reference points were provided by classical literature. The developments of radiocarbon dating and dendrochronology have done much to further knowledge in this area.

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